Ku-Band radar penetration into Snow over Arctic Sea Ice

Sea ice freeboard measurements are of great interest for basin-scale ice mass balance monitoring. Typically, laser- and radar-altimeters are used for freeboard retrieval in operational systems such as aircrafts and satellites. For laser beams it can be assumed that the dominant reflector is the snow...

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Main Authors: Hendricks, Stefan, Stenseng, Lars, Helm, Veit, Hanson, Susanne, Haas, Christian
Format: Conference Object
Language:English
Published: 2009
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/659bc06f-9d9b-4411-91a4-8a63fbd61ed8
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spelling ftdtupubl:oai:pure.atira.dk:publications/659bc06f-9d9b-4411-91a4-8a63fbd61ed8 2023-05-15T14:24:09+02:00 Ku-Band radar penetration into Snow over Arctic Sea Ice Hendricks, Stefan Stenseng, Lars Helm, Veit Hanson, Susanne Haas, Christian 2009 https://orbit.dtu.dk/en/publications/659bc06f-9d9b-4411-91a4-8a63fbd61ed8 eng eng info:eu-repo/semantics/restrictedAccess Hendricks , S , Stenseng , L , Helm , V , Hanson , S & Haas , C 2009 , ' Ku-Band radar penetration into Snow over Arctic Sea Ice ' , 2009 AGU Fall Meeting , San Fransisco, CA , United States , 14/12/2009 - 18/12/2009 . conferenceObject 2009 ftdtupubl 2022-08-14T07:47:33Z Sea ice freeboard measurements are of great interest for basin-scale ice mass balance monitoring. Typically, laser- and radar-altimeters are used for freeboard retrieval in operational systems such as aircrafts and satellites. For laser beams it can be assumed that the dominant reflector is the snow/air interface, whereas radar waves interact with the variable physical properties of the snow cover on the Arctic sea ice. In addition, radar elevation measurements may vary for different retracker algorithms, which determine the track point of the scattered echo power distribution. Since accurate knowledge of the reflection horizon is critical for sea ice thickness retrieval, validation data is necessary to investigate the penetration of radar waves into the snow for the upcoming CryoSat-2 mission. Furthermore, the combination of both optical and RF wavelengths might be used to derive snow thickness, if radar altimeters are capable of measuring the distance to the snow-ice interface reliably. We present the results of aircraft campaigns in the Arctic with a scanning laser altimeter and the Airborne SAR/Interferometric Radar Altimeter System (ASIRAS) of the European Space Agency. The elevation observations are converted into freeboard profiles, taking the different footprints into account when comparing the two systems. Based on the probability distribution of laser and radar freeboard we discuss the specific characteristics of both systems and the apparent radar penetration over sea ice in the northern Baltic Sea, the Greenland and Lincoln Sea. The results show differences in the penetration of Ku-Band radar between regions and interannual variability. In general, snow thickness could not be derived in the Arctic, whereas the penetration behavior correlates with other (QuikScat) remote sensing products. Conference Object Arctic Arctic Greenland Lincoln Sea Sea ice Technical University of Denmark: DTU Orbit Arctic Greenland
institution Open Polar
collection Technical University of Denmark: DTU Orbit
op_collection_id ftdtupubl
language English
description Sea ice freeboard measurements are of great interest for basin-scale ice mass balance monitoring. Typically, laser- and radar-altimeters are used for freeboard retrieval in operational systems such as aircrafts and satellites. For laser beams it can be assumed that the dominant reflector is the snow/air interface, whereas radar waves interact with the variable physical properties of the snow cover on the Arctic sea ice. In addition, radar elevation measurements may vary for different retracker algorithms, which determine the track point of the scattered echo power distribution. Since accurate knowledge of the reflection horizon is critical for sea ice thickness retrieval, validation data is necessary to investigate the penetration of radar waves into the snow for the upcoming CryoSat-2 mission. Furthermore, the combination of both optical and RF wavelengths might be used to derive snow thickness, if radar altimeters are capable of measuring the distance to the snow-ice interface reliably. We present the results of aircraft campaigns in the Arctic with a scanning laser altimeter and the Airborne SAR/Interferometric Radar Altimeter System (ASIRAS) of the European Space Agency. The elevation observations are converted into freeboard profiles, taking the different footprints into account when comparing the two systems. Based on the probability distribution of laser and radar freeboard we discuss the specific characteristics of both systems and the apparent radar penetration over sea ice in the northern Baltic Sea, the Greenland and Lincoln Sea. The results show differences in the penetration of Ku-Band radar between regions and interannual variability. In general, snow thickness could not be derived in the Arctic, whereas the penetration behavior correlates with other (QuikScat) remote sensing products.
format Conference Object
author Hendricks, Stefan
Stenseng, Lars
Helm, Veit
Hanson, Susanne
Haas, Christian
spellingShingle Hendricks, Stefan
Stenseng, Lars
Helm, Veit
Hanson, Susanne
Haas, Christian
Ku-Band radar penetration into Snow over Arctic Sea Ice
author_facet Hendricks, Stefan
Stenseng, Lars
Helm, Veit
Hanson, Susanne
Haas, Christian
author_sort Hendricks, Stefan
title Ku-Band radar penetration into Snow over Arctic Sea Ice
title_short Ku-Band radar penetration into Snow over Arctic Sea Ice
title_full Ku-Band radar penetration into Snow over Arctic Sea Ice
title_fullStr Ku-Band radar penetration into Snow over Arctic Sea Ice
title_full_unstemmed Ku-Band radar penetration into Snow over Arctic Sea Ice
title_sort ku-band radar penetration into snow over arctic sea ice
publishDate 2009
url https://orbit.dtu.dk/en/publications/659bc06f-9d9b-4411-91a4-8a63fbd61ed8
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Arctic
Greenland
Lincoln Sea
Sea ice
genre_facet Arctic
Arctic
Greenland
Lincoln Sea
Sea ice
op_source Hendricks , S , Stenseng , L , Helm , V , Hanson , S & Haas , C 2009 , ' Ku-Band radar penetration into Snow over Arctic Sea Ice ' , 2009 AGU Fall Meeting , San Fransisco, CA , United States , 14/12/2009 - 18/12/2009 .
op_rights info:eu-repo/semantics/restrictedAccess
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